These new seismic stations will have two major components-- Strong Motion Accelerograph (SMA) and another is Broadband Seismometer (BBS), said senior scientist of ISR Dr Santosh Kumar.
At present, there are 60 permanent stations having such sensors in Gujarat as part of the earthquake early warning system. Out of these 60 stations, 45 are directly connected with ISR while remaining are offline.
According to Kumar, the 50 new stations will collect and analyse various noises, seismic waves and signals coming from the crust of the earth, which will help the scientists to locate active fault-lines which are responsible for earthquakes.
"ISR has planned to set up 50 new seismic stations to study what is happening below the surface of Gujarat. The main purpose of this project is to find out what is going on in deep mantle or deep crust by analysing various noises coming out from the earth" said Kumar.
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Broadband Seismometers are instruments that measure motion of the ground including those of seismic waves generated by earthquakes, volcanic eruptions and other seismic sources.
Records of seismic waves allow seismologists to map the interior of the Earth as well as to locate and measure the size of these different sources. Strong Motion Accelerographs are useful when the earthquake ground motion is so strong that it causes the more sensitive seismometers to go off-scale, said Kumar.
"In this way we will have every minute detail of each
place. This exercise will continue until data of entire state is collected. Through this, we can locate active fault lines at micro level," said Kumar.
Describing the need for such a project, he said that Gujarat is very different from other regions in India, as minor earthquakes keep striking, which is a unique phenomena.
"There is very less information about what is lying beneath Gujarat's earth. Gujarat is different from others as we continuously get minor earthquakes even after the major earthquake of 2001. We have to probe why Gujarat's crust is so much active," said Kumar.
"This new project will work as an MRI scan of earth's crust. It will tell us where these faultlines are located and what they are capable of. In the long run, it will help us in estimating or predicting long term seismic hazard here," said Kumar.